2026-08-05T08:38:41Zhttp://doidb.wdc-terra.org/oaip/oai

oai:doidb.wdc-terra.org:70762025-03-06T12:27:29ZDOIDBDOIDB.SEISNET

false4DOIDB.SEISNET 10.14470/9B7563261622 Yu, Changqing Key Laboratory of Deep-Earth Dynamics of Ministry of Natural Resources, Institute of Geology, Chinese Academy of Geological Sciences, Beijing, China Mechie, James Deutsches GeoForschungsZentrum, Potsdam, Germany GFZ Data Services 2021 Deutsches GeoForschungsZentrum GFZ GEOFON Data Centre geofon@gfz.de Geophysical Instrument Pool Potsdam (GIPP) Key Laboratory of Deep-Earth Dynamics of Ministry of Natural Resources, Institute of Geology, Chinese Academy of Geological Sciences, Beijing, China Deutsches GeoForschungsZentrum – GFZ, Section “Geophysical Imaging“, Potsdam, Germany Receiver functions Mantle structure Monitoring system EARTH SCIENCE > SOLID EARTH In Situ/Laboratory Instruments > Magnetic/Motion Sensors > Seismometers In Situ Land-based Platforms > GEOPHYSICAL STATIONS/NETWORKS In Situ Land-based Platforms > GEOPHYSICAL STATIONS/NETWORKS > SEISMOLOGICAL STATIONS Geophysics Passive seismic Seismometers Velocity MiniSEED GIPP MESI Crustal Temporary 2018-05-01 2018-05-01 2021-04-01 2024-02-01 en Seismic Network embargoed access Creative Commons Attribution-NoDerivatives 4.0 International https://geofon.gfz.de/waveform/archive/response/4O/2018_2020 868GB .mseed XML The main aim of this project is to investigate the crustal and mantle structure beneath the Longmenshan fault zone in China, based on a very dense passive seismology profile. The Longmenshan fault zone hosted the Wenchuan earthquake of May 2008 with a magnitude (Mw) of 7.9 and the Lushan earthquake of June 2013 with a magnitude (Mw) of 6.6. It is planned to mainly use the receiver-function method, to investigate the crustal and mantle structure beneath the Longmenshan fault zone. Waveform data are available from the GEOFON data center, under network code 4O. 102.0 105.0 30.0 33.0 China GFZ Helmholtz Centre for Geosciences https://ror.org/04z8jg394 GIPP201801